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Gruber P. Convex and Discrete Geometry

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15 Combinatorial Theory of <strong>Convex</strong> Polytopes 271<br />

For additional information the reader may consult the books of Grünbaum [453],<br />

Ziegler [1045], Richter-Gebert [833] <strong>and</strong> Matouˇsek [695] <strong>and</strong> the surveys of Bayer<br />

<strong>and</strong> Lee [83] <strong>and</strong> Kalai [561].<br />

Steinitz’ Representation Theorem for <strong>Convex</strong> Polytopes in E 3<br />

We shall prove the following basic result.<br />

Theorem 15.6. Let G be a planar 3-connected graph. Then G is isomorphic to the<br />

edge graph of a convex polytope in E 3 .<br />

Proof. For terminology, see Sect. 34.1. An application of the Koebe–Brightwell–<br />

Scheinerman theorem 34.1 together with a suitable Möbius transformation <strong>and</strong> stereographic<br />

projection shows that there is a primal-dual circle representation of G on the<br />

unit sphere S 2 with the following properties.<br />

The country circle of the outer country is the equator.<br />

All other country circles are in the southern hemisphere.<br />

Three of these touch the equator at points which are 2π 3 apart.<br />

From now on we use this primal-dual circle representation of G.<br />

For each country circle choose a closed halfspace with the country circle in its<br />

boundary plane such that the halfspace of the equator circle contains the south pole<br />

of S 2 <strong>and</strong> the other halfspaces the origin o. The intersection of these halfspaces is<br />

then a convex polytope P. The countries, resp. the country circles of G correspond<br />

to the facets of P. Letv ∈ S 2 be a vertex (of the representation) of G on S 2 .The<br />

country circles of the countries with vertex v form a ring around v like a string<br />

of beads, possibly of different sizes, on the vertex circle of v. The latter intersects<br />

these country circles orthogonally. All other country circles are outside this ring.<br />

This shows that the boundary planes of the halfspaces corresponding to the circles<br />

of the ring meet in a point v P, say, radially above v <strong>and</strong> v P is an interior point of all<br />

other halfspaces. Thus v P is a vertex of P. IfC is a country circle of the ring, the<br />

facet F of P determined by C has two edges which contain v P <strong>and</strong> are tangent to C<br />

<strong>and</strong> thus to S 2 .Ifvw···z is a cycle of G around C, then v PwP ···z P is a cycle of<br />

edges of F <strong>and</strong> thus is the cycle of edges of F. Each edge of F is tangent to S 2 at<br />

the point where it touches the incircle C of F. Since, by construction, the edge graph<br />

of P is obtained by radial projection of the representation of G (in S 2 ), the proof is<br />

complete. ⊓⊔<br />

Different Ways to Represent a <strong>Convex</strong> Polytope<br />

The above proof of the Steinitz representation theorem shows that any convex polytope<br />

in E 3 is (combinatorially) isomorphic to a convex polytope all edges of which<br />

touch the unit ball B 3 . A far-reaching generalization of this result is due to Schramm<br />

[914] in which B 3 is replaced by any smooth <strong>and</strong> strictly convex body in E 3 .

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